生态环境学报 ›› 2025, Vol. 34 ›› Issue (6): 931-940.DOI: 10.16258/j.cnki.1674-5906.2025.06.010

• 研究论文【环境科学】 • 上一篇    下一篇

水动力作用下河道底泥氨氮释放特性分析

任宸剑1(), 郝瑞霞1,3, 张杨2, 韩丽娟1,3,*(), 魏煜星1, 柴璐1   

  1. 1.太原理工大学水利科学与工程学院,山西 太原 030000
    2.山西省水利发展中心,山西 太原 030000
    3.流域水资源协同利用山西省重点实验室,山西 太原 030000
  • 收稿日期:2024-10-20 出版日期:2025-06-18 发布日期:2025-06-11
  • 通讯作者: * 韩丽娟, E-mail: hanlijuan@tyut.edu.cn
  • 作者简介:任宸剑(1999年生),女,硕士研究生,主要从事水力学及河流动力学研究。E-mail: 972909938@qq.com
  • 基金资助:
    山西省基础研究项目(202103021223079);长江科学院开放基金项目(CKWV2021869/KY);山西省回国留学人员科研资助项目(2021-051);山西省水利科学技术研究与推广项目(2022GM017);国家自然科学基金项目(52109099)

The Release Characteristics of Ammonia Nitrogen from River Sediments Driven by Hydrodynamic Forces

REN Chenjian1(), HAO Ruixia1,3, ZHANG Yang2, HAN Lijuan1,3,*(), WEI Yuxing1, CHAI Lu1   

  1. 1. College of Water Conservancy Science and Engineering, Taiyuan University of Technology, Taiyuan 030000, P. R. China
    2. Shanxi Water Conservancy Development Center, Taiyuan 030002, P. R. China
    3. Shanxi Key Laboratory of Collaborative Utilization of River Basin Water Resources, Taiyuan 030000, P. R. China
  • Received:2024-10-20 Online:2025-06-18 Published:2025-06-11

摘要:

氨氮是引起河道富营养化的重要原因,了解水动力条件下河道底泥中氨氮的释放特性对了解河流水质的动态至关重要。为探究水动力作用对河道底泥起动与氨氮释放规律的影响,于汾河太原段下游取样开展室内实验,研究恒定和变化水动力条件下底泥再悬浮与氨氮浓度的时空变化以及释放速率等,构建不同强度水动力作用下近底切应力与底泥起动、上覆水浊度、氨氮浓度的相关关系。结果表明,水动力条件变化引起的近底切应力变化是影响上覆水浊度和氨氮浓度的关键因素。当近底切应力为1.07 N·m−2时,中值粒径d50=0.020 mm的底泥达到“普遍动”的起动状态,底泥向上覆水中大量悬浮;氨氮在扰动初期释放速率最快,前60 min氨氮释放量占总释放量的60.4%;当近底切应力小于0.260 N·m−2时,氨氮浓度在实验初期释放存在分层现象,底部氨氮浓度处于较高的水平,随着转速的增加和时间的推移(180 min后)垂向上氨氮浓度趋于一致;上覆水浊度和氨氮浓度随底泥面切应力的增加而增加,越强的水动力条件越有助于提高上覆水中氨氮浓度的阈值上限,该研究中氨氮质量浓度和释放速率最大值分别为0.569 mg·L−1、249 mg·m−2·d−1;近底切应力与底泥向上覆水释放的氨氮浓度呈线性增加关系,与水体浊度呈近似指数增加关系。

关键词: 底泥再悬浮, 水力扰动, 氨氮浓度, 内源污染, 河道水质治理

Abstract:

Ammonia nitrogen is a pivotal contributor to the eutrophication of aquatic ecosystems. Understanding the release mechanisms of ammonia nitrogen from river sediments under varying hydrodynamic conditions is essential for effective management of water quality. This study investigated the effects of hydrodynamic forces on sediment resuspension and the release dynamics of ammonia nitrogen by using sediment samples collected from the downstream section of the Fenhe River in Taiyuan. Laboratory experiments were conducted to analyze the spatiotemporal variations in sediment resuspension and ammonia nitrogen concentration under steady and dynamic hydrodynamic conditions as well as the associated release rates. Correlations were established between near-bottom shear stress, sediment resuspension, overlying water turbidity, and ammonia nitrogen concentration under different intensities of hydrodynamic disturbance. The results revealed that the near-bottom shear stress is a key determinant of turbidity and ammonia nitrogen concentration in the overlying water. When the near-bottom shear stress reached 1.065 N·m−2, sediment with a median particle size (d50) of 0.020 mm transitioned into a state of “general motion,” resulting in significant sediment resuspension. The release rate of ammonia nitrogen was highest during the initial disturbance phase, with 60.4% of the total ammonia nitrogen released within the first 60 min. When the near-bottom shear stress was below 0.260 N·m−2, the ammonia-nitrogen concentration exhibited stratification during the initial phase of the experiment, with higher concentrations near the sediment layer. However, the vertical concentration became more uniform after 180 min. Both turbidity and ammonia nitrogen concentration in the overlying water increased with increasing shear stress on the sediment surface. Stronger hydrodynamic conditions facilitated higher thresholds of ammonia-nitrogen concentrations in the overlying water. The maximum ammonia nitrogen concentration and release rate observed in this study were 0.569 mg·L−1 and 249.19 mg·m−2·d−1, respectively. A linear relationship was observed between the near-bottom shear stress and ammonia nitrogen concentration released into the overlying water, whereas turbidity exhibited an approximately exponential increase with increasing shear stress.

Key words: sediment resuspension, hydrodynamic disturbance, ammonia nitrogen concentration, internal pollution, river water quality management

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